Nature and Age of Detrital Zircons from Rocks of the Shear Zone: The Problem of Occurrence of the Archean Basement in the Transangarian Yenisei Ridge

I. I. Likhanov; P. S. Kozlov; V. V. Reverdatto; N. V. Popov

doi:10.1134/S1028334X18050161

Nature and Age of Detrital Zircons from Rocks of the Shear Zone: The Problem of Occurrence of the Archean Basement in the Transangarian Yenisei Ridge

Авторлар: Likhanov I.I.¹, Kozlov P.S.², Reverdatto V.V.¹, Popov N.V.³
Мекемелер:
1. Sobolev Institute of Geology and Mineralogy, Siberian Branch
2. Zavaritskii Institute of Geology and Geochemistry, Ural Branch
3. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch
Шығарылым: Том 480, № 1 (2018)
Беттер: 568-572
Бөлім: Geology
URL: https://ogarev-online.ru/1028-334X/article/view/193018
DOI: https://doi.org/10.1134/S1028334X18050161
ID: 193018

Дәйексөз келтіру

Толық мәтін

Ашық рұқсат
Рұқсат жабық

Рұқсат берілді
Рұқсат жабық

Тек жазылушылар үшін

Аннотация
Авторлар туралы
Әдебиет тізімі
Қосымша файлдар
Статистика

Аннотация

Petrogeochemical and geochronological study of boudined quartzite sandstones and tonalites, as well as host amphibolites, in the shear zone showed that potential sources of detrital zircons were Neoarchean–Paleoproterozoic rocks of the Angara–Kan block and products of their metamorphism. Interpretation of the available data does not confirm the inferred presence of the Early Precambrian basement of the Siberian Craton in the Transangara region.